Holocene vegetation change in relation to fire and volcanic events in Jilin, Northeastern China

• Published in: Science China Earth Sciences
• Main Authors: Zhao HongLi, Li XiaoQiang, Hall, Valerie A.
• Format: Article in Journal/Newspaper
• Language: English
• Published: SCIENCE PRESS 2015
• Subjects: Holocene; Vegetation Change; Fire History; Tephra Shards; Volcanic Events; Northeastern China; Science & Technology; Physical Sciences; Sihailongwan Maar Lake; Baitoushan Volcano; Volatile Emission; Pollen Record; Ne China; Ice Core; Eruption; Charcoal; Sediments; History; Geology; Geosciences; Multidisciplinary; ice core
• Online Access: http://ir.ieecas.cn/handle/361006/9275; http://ir.ieecas.cn/handle/361006/9276; https://doi.org/10.1007/s11430-015-5068-8

Volatiles erupted from large-scale explosive volcanic activities have a significant impact on climate and environmental changes. As an important ecological factor, the occurrence of fire is affected by vegetation cover, and fire can feed back into both vegetation and climatic change. The causes of fire events are diverse; and can include volcanic eruptions. The amount of charcoal in sediment sequences is related to the frequency and intensity of fire, and hence under good preservation conditions fire history can be reconstructed from fossil charcoal abundance. Until now, little research on the role of fire has been carried out in northeastern China. In this study, through research on charcoal and tephra shards from Gushantun and Hanlongwan, Holocene vegetation change in relation to fire and volcanic events in Jilin, Northeastern China, was investigated. Where tephra shards are present in Gushantun it is associated with low level of both conifers and broadleaved trees, and is also associated with a pronounced charcoal peak. This suggests forest cover was greatly reduced from a fire caused by an eruption of the Tianchi volcano. We also detected one tephra layer in Hanlongwan, which also has the almost same depth with low level forest pollen values and one charcoal peak. This was caused probably by an eruption of the Jinlongdingzi volcano.